Carbon emission from permafrost soils underestimated by 14%

Date:
June 15, 2020
Source:
University of Michigan
Summary:
Picture 500 million cars stacked in rows. That's how much carbon
-- about 1,000 petagrams, or one billion metric tons - -is locked
away in Arctic permafrost.



FULL STORY ========================================================================== Picture 500 million cars stacked in rows. That's how much carbon --
about 1,000 petagrams, or one billion metric tons -- is locked away in
Arctic permafrost.


========================================================================== Currently, scientists estimate that 5-15% of the carbon stored in surface permafrost soils could be emitted as the greenhouse gas carbon dioxide
by 2100, given the current trajectory of global warming. This emission,
spurred by microbial action, could lead to 0.3 to 0.4 degrees Celsius
of additional global warming.

But this estimation is missing a crucial path that carbon dioxide may
be entering the atmosphere: sunlight.

According to a University of Michigan study, organic carbon in thawing permafrost soils flushed into lakes and rivers can be converted to carbon dioxide by sunlight, a process known as photomineralization.

The research, led by aquatic geochemist Rose Cory, has found
that organic carbon from thawing permafrost is highly susceptible
to photomineralization by ultraviolet and visible light, and could
contribute an additional 14% of carbon dioxide into the atmosphere. Her
team's study is published in the journal Geophysical Research Letters.

"Only recently have global climate models included greenhouse gases from thawing permafrost soils. But none of them contain this feedback pathway,"
said Cory, an associate professor of earth and environmental sciences.



==========================================================================
"To get a number on how much carbon could be released from permafrost
soils through oxidation, we have to understand what are the processes and
what is the timescale: maybe this carbon is just so resistant to oxidation that, even if thawed out, it would just flow into the Arctic ocean and
be buried in another freezer." This pathway has been debated because
measuring how sunlight degrades soil carbon is difficult. Each wavelength
of light has a different effect on soil organic carbon, as does the level
of iron in the soil. To precisely measure how carbon dioxide is emitted
when organic carbon is exposed to sunlight, Cory's co-corresponding
author Collin Ward, a scientist at Woods Hole Oceanographic Institution
and U-M alum, developed a method to measure each wavelength's effect
on soil organic carbon. To do this, he built a new instrument that uses
LED lights to mimic different wavelengths of the sun.

"This new LED-based method makes it far easier and cheaper to figure out
how light-driven reactions vary for different wavelengths of the sun,"
Ward said.

"After I built the instrument I immediately called Rose and told her that
I wanted to first use it on permafrost samples." The researchers placed organic carbon leached from soil samples from six Arctic locations in
the instrument, and then subjected the samples to the LED light.

After the light exposure, they extracted the carbon dioxide cryogenically
and used a mass spectrometer to measure the age and amount of carbon
dioxide given off by the soil carbon.

They found that not only did the wavelength of sunlight impact the
amount of carbon dioxide released, the amount of iron in the sample did
as well. Iron acted as a catalyst, increasing the reactivity of the soil.



========================================================================== "What we have long suspected is that iron catalyzes this sunlight-driven process, and that's exactly what our results show," Cory said. "As the
total amount of iron increases, the amount of carbon dioxide increases."
Cory's team also used carbon dating to age the soil organic carbon and
the carbon dioxide emitted from it to demonstrate this oxidation was
happening to ancient permafrost, not just soil that thaws annually. This
is important because soil that thaws annually would release a much
smaller amount of carbon dioxide than what's available in permafrost.

The researchers found that it was between 4,000 and 6,300 years old,
and by demonstrating how old the soil is, they show that permafrost
carbon is susceptible, or labile, to oxidation to carbon dioxide.

"Not only do we have the first wavelength specific measurement of this sunlight-driven reaction but we have verification that it's old carbon
that is oxidized to carbon dioxide," Cory said. "We can put to rest
any doubt that sunlight will oxidize old carbon and we show what is
controlling this process - - it's the iron that catalyzes the sunlight oxidation of ancient (or old) carbon." Including the U-M team's
finding into climate change models means that - - conservatively --
there could be a release of 6% of the 100 billion metric tons of carbon currently stored in Arctic permafrost. If 6% doesn't sound like much,
consider that's the carbon equivalent of approximately 29 million cars evaporating into the atmosphere.


========================================================================== Story Source: Materials provided by University_of_Michigan. Note:
Content may be edited for style and length.


========================================================================== Journal Reference:
1. J. C. Bowen, C. P. Ward, G. W. Kling, R. M. Cory. Arctic
amplification of
global warming strengthened by sunlight oxidation of permafrost
carbon to CO 2. Geophysical Research Letters, 2020; DOI:
10.1029/2020GL087085 ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2020/06/200615140854.htm

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